Determination of the averaged charge-to-mass ratio of the heavy charged constituents of a magnetoplasma using whistler wave measurements

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Abstract

In a cold magnetized plasma with two light ions of comparable gyrofrequencies and any species of heavy ions and/or charged dust particulates, a technique is developed to recover the relative charge density of the heavy plasma population and to estimate its effective averaged charge-to-mass ratio. Such results can be obtained without using mass spectrometer data but only the measurements of the ion plasma frequency, the electron gyro- and plasma frequencies as well as the two highest ion cutoff frequencies. © Author(s) 2010.

Figures

  • Fig. 1a. Altitude profiles of the relative charge densities of the three ion species H+, O+ and Cs+, as well as of the normalized averaged gyrofrequency 〈ωIPB〉/ωCs+ . The IPB is formed by Cs + ions which contaminate the ionospheric background plasma constituted by the two light ions H+ and O+ distributed in altitude according to a diffusive equilibrium type model. The solid lines show the corresponding values of νO+ and νH+ , taking into account that the assumed contamination by the Cs+ ions does not depend on the altitude, whereas the superposed stars correspond to calculations based on Eq. (13). The dotted (resp. dashed) lines represent the recovered relative charge density νCs+ and normalized averaged gyrofrequency of the IPB, 〈ωIPB〉/ωCs+ , respectively; (a) and (b) correspond to different levels of plasma contamination: (a) νCs+ = 0.2; (b) νCs+ = 0.5.
  • Fig. 1b. νCs+ = 0.5.
  • Fig. 2. Curves similar to those of Fig. 1, but for a plasma contamination by negative CS−4 ions of relative charge density νCS−4 = 0.2.

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APA

Krafft, C., & Lundin, B. V. (2010). Determination of the averaged charge-to-mass ratio of the heavy charged constituents of a magnetoplasma using whistler wave measurements. Annales Geophysicae, 28(12), 2237–2247. https://doi.org/10.5194/angeo-28-2237-2010

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